Data

TOPEX/POSEIDON Altimeter Sea Surface Height Anomaly (SSHA)

Tasmanian Partnership for Advanced Computing
Dr Edward King (Managed by)
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ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Adc&rfr_id=info%3Asid%2FANDS&rft_id=http://dl.tpac.org.au/tpacportal/#dataset=26&rft.title=TOPEX/POSEIDON Altimeter Sea Surface Height Anomaly (SSHA)&rft.identifier=dl.tpac.org.au/ds/26&rft.publisher=Tasmanian Partnership for Advanced Computing&rft.description=This dataset has the along-track sea surface height anomalies (SSHA) for the TOPEX/Poseidon mission up to the time of its orbit change (September, 1992 - August, 2002; cycles 1-365). The data from after the orbit change (September, 2002 - September, 2005) are available elsewhere. The dual-frequency NASA radar altimeter, NRA, is the primary instrument of the TOPEX/Poseidon mission. It works by sending radio pulses at 13.6 GHz and 5.3 GHz toward the earth and measuring the characteristics of the echo. By combining this measurement with data from the microwave radiometer and with other information from the spacecraft and the ground, scientists can calculate the height of the sea surface to within 4.3 centimeters. The data have been corrected for path delay effects (wet- and dry-troposphere, ionosphere, sea-state bias), for tides, and for the inverse barometer effect.&rft.creator=Jet Propulsion Laboratory of California Institute of Technology&rft.date=2012&rft.coverage=northlimit=0; southlimit=-180; westlimit=-66; eastLimit=66; projection=WGS84&rft_subject=Physical Oceanography&rft_subject=EARTH SCIENCES&rft_subject=OCEANOGRAPHY&rft.type=dataset&rft.language=English Access the data

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Brief description

This dataset has the along-track sea surface height anomalies (SSHA) for the TOPEX/Poseidon mission up to the time of its orbit change (September, 1992 - August, 2002; cycles 1-365). The data from after the orbit change (September, 2002 - September, 2005) are available elsewhere. The dual-frequency NASA radar altimeter, NRA, is the primary instrument of the TOPEX/Poseidon mission. It works by sending radio pulses at 13.6 GHz and 5.3 GHz toward the earth and measuring the characteristics of the echo. By combining this measurement with data from the microwave radiometer and with other information from the spacecraft and the ground, scientists can calculate the height of the sea surface to within 4.3 centimeters. The data have been corrected for "path delay" effects (wet- and dry-troposphere, ionosphere, sea-state bias), for tides, and for the inverse barometer effect.

Data time period: 09 1992 to 31 08 2002

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Oceans

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Identifiers
  • Local : dl.tpac.org.au/ds/26